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2900 - Site Mitigation Program
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PR0542431
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Last modified
5/4/2020 4:08:39 PM
Creation date
5/4/2020 3:35:21 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0542431
PE
2960
FACILITY_ID
FA0024384
FACILITY_NAME
PORT OF STOCKTON CARGILL PROP
STREET_NUMBER
0
STREET_NAME
PORT
STREET_TYPE
RD
City
STOCKTON
Zip
95203
APN
14503012
CURRENT_STATUS
01
SITE_LOCATION
PORT RD 21
QC Status
Approved
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EHD - Public
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r <br /> 4.1.1 Soil Analysis <br /> Soil sample SB1-1 was analyzed for pH, hydrocarbons and Benzene, Toluene, Ethylbenzene and <br /> Xylene (BTEX) utilizing U.S. Environmental Protection Agency (EPA) approved analysis <br /> ' methods. Analysis of these samples revealed them to be nondetected to their respective detection <br /> limits. <br /> A copy of the analysis report, along with Chain-of-Custody documentation for these samples, is <br /> included in Appendix A of this report. <br /> A copy of the soil boring is included as Appendix B of this report. <br /> 4.2 GROUNDWATER MONITORING WELL INSTALLATION <br /> On November 22, 1991, IT installed one groundwater monitoring well on the subject property. <br /> The well was drilled at the southern extent of the property, directly south of the aforementioned <br /> soil boring (see Figure 2). The purpose of this well was to assess possible migration of potential <br /> soil and/or groundwater contamination caused by known leaking USTs in the area. <br /> Groundwater gradient maps for this site were not available. Because of the close proximity of <br /> the Stockton Deep Water Shipping Channel, shallow groundwater was assumed to flow south to <br /> north. Based on this assumption, the subject property was determined to be down-gradient of at <br /> least one known leaking UST and therefore, it was chosen as the best location to assess the <br /> possible groundwater impact. <br /> The groundwater monitoring well was installed using a hollow-stemmed auger. This allowed <br /> collection of soil samples during the well installation in the same manner as used for the soil <br /> boring. Soil samples were collected at five foot intervals down to the completed well depth. The <br /> water table was encountered at 12.0 feet below surface at the well location. An OVA was <br /> utilized to screen the samples for analysis. Since no readings above background were detected <br /> with the instrument, the soil sample collected at the 10 foot interval was submitted for analysis <br /> to the PACE Laboratory in Novato, California. <br /> 3 <br /> WAI M9 I/EES/L7R:0817.IP! <br />
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